Nitrogen (Ammonia) N · 7

Nitrogen pulled out of the air and joined to hydrogen under pressure — the invention that roughly doubled how many people the planet can feed.

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Ammonia synthesis consumes on the order of one to two percent of world energy and is the reason synthetic fertiliser exists at all.

Where it is in the Earth

Nitrogen is not mined from a deposit in any conventional sense. It does not accumulate in a vein, a seam, or a sedimentary bed the way iron or potash do. Instead, the raw material is the air itself, which is approximately four-fifths nitrogen by volume. The challenge has never been scarcity of the element — nitrogen is the most abundant gas in the atmosphere — but rather the extraordinary stability of the nitrogen molecule. Two nitrogen atoms are held together by a triple bond, one of the strongest in common chemistry, which makes atmospheric nitrogen almost entirely inert. Plants and most other organisms cannot use it in that form.

The geological story of nitrogen as a resource is therefore really the story of a fixation problem. In nature, lightning and certain soil bacteria break that triple bond and convert atmospheric nitrogen into compounds — nitrates, ammonium — that living things can absorb. Before the twentieth century, agriculture depended on these natural pathways plus deposits of sodium nitrate, called caliche, found in the Atacama Desert of Chile, where extraordinarily dry conditions preserved ancient accumulations of oxidised nitrogen compounds in surface rocks. Those Chilean deposits were the world's principal source of fixed nitrogen for fertiliser and explosives until a synthetic alternative arrived.

The synthetic alternative is the Haber-Bosch process, developed in the early twentieth century, which uses high pressure and temperature together with an iron catalyst to force atmospheric nitrogen to react with hydrogen and form ammonia (NH₃). From that point on, the limiting factor on nitrogen supply shifted from geology to energy and hydrogen supply. Modern ammonia plants are built near natural gas pipelines, not near ore deposits, because the hydrogen comes almost entirely from natural gas through a process called steam methane reforming. The nitrogen still comes from air, separated at the plant. There is no ore grade to speak of and no overburden to move.

Getting it out

Because ammonia synthesis draws its nitrogen from the atmosphere, there is no mine in the usual sense. Air separation units — large industrial installations that cool air until it liquefies and then fractionate it by the different boiling points of its components — deliver essentially pure nitrogen gas to the synthesis section of the plant. This is an industrial rather than an extractive operation, and the concept of ore grade or strip ratio does not apply to it.

The meaningful extraction step is on the hydrogen side. Most hydrogen used in ammonia production today comes from natural gas, and that gas is produced through conventional well drilling and gathering. Where coal is used as the hydrogen feedstock, as is common in China, it arrives via coal mining. The energy intensity of getting hydrogen to the plant — and the carbon footprint that comes with it — is where the economics and the environmental discussion actually live. A smaller share of global ammonia is made using hydrogen from coal gasification, naphtha reforming, or, in a growing number of announced projects, electrolysis powered by renewable electricity, though the last of these remains a small fraction of current output.

The only remnant of conventional mining in the nitrogen supply chain is the Chilean caliche, which still produces some natural nitrates used in speciality applications. That material is mined by open-pit methods from surface and near-surface horizons in the Atacama, but it plays no material role in global nitrogen supply compared with synthetic ammonia. The practical result is that the nitrogen supply chain carries almost none of the geological concentration risk that surrounds metals or even phosphate, but it carries very large energy and feedstock risks instead.

What pulls on it

The overwhelming share of ammonia production goes into fertiliser, and the reason is straightforward: nitrogen is the element most commonly limiting to plant growth in agricultural soils. Crops remove nitrogen from the soil every harvest, and without replenishment yields fall. The three principal fertiliser products — urea, ammonium nitrate, and ammonium sulfate — deliver that nitrogen in forms crops can absorb. The global population and the dietary shift in growing economies toward more meat, which requires more grain per calorie, have together kept fertiliser nitrogen demand on a long upward trend.

Outside agriculture, ammonia feeds into industrial applications including the production of plastics, fibres such as nylon, explosives for mining and construction, and cleaning products. These non-agricultural uses are substantial in absolute terms but small relative to the fertiliser fraction. A newer and actively discussed demand category is ammonia as a carrier for hydrogen in low-carbon shipping and power generation: because ammonia can be liquefied at moderate pressure and has a reasonable energy density, it is being evaluated as a way to ship hydrogen produced in one region to consumers in another, without the extreme refrigeration that liquid hydrogen itself requires. This pathway is not yet a material contributor to demand, but engineering and infrastructure choices being made now will determine whether it becomes one over the coming decades.

Demand would shift sharply if agricultural practice changed at scale — for instance, if biological nitrogen fixation by engineered crops or soil microbes became capable of replacing synthetic inputs, or if food systems contracted. Neither appears imminent. On the energy-carrier side, demand growth depends on policy commitments, the cost trajectory of green hydrogen, and port infrastructure investment that has not yet been made in most regions. The fertiliser demand base, by contrast, is tied to the number of people eating and to the productivity of farmland, both of which change slowly.